Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/10694
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dc.date.accessioned2018-02-15T10:56:29Zen
dc.date.available2018-02-15T10:56:29Zen
dc.date.issued2018-01en
dc.identifier.urihttp://hdl.handle.net/2122/10694en
dc.description.abstractParsons et al. (2012), compared the characteristic and Gutenberg–Richter (G-R) distributions for time-dependent M ≥ 7.9 earthquake probability in the Nankai-Tokai subduction zone, Japan, a region for which historical information about several repeating strong earthquakes does exist. The purpose of their paper was to assess the possibility of making reasonable hazard assessments without requiring a characteristic model, and the conclusion was yes. In fact, they found that a simulator that imposes no physical geometric rupture barriers (meaning gaps or steps in the faults), can replicate the spatial proportion of fault segment ruptures evident within the studied area (within 95% confidence bounds). They concluded that the adoption of a G-R model can attain very similar matches to the historical catalog of the Nankai-Tokai zone, and suggested that very simple earthquake rupture simulations based on empirical data and fundamental earthquake laws could be useful forecast tools in information-poor settings.en
dc.language.isoEnglishen
dc.relation.ispartofPhysics of the Earth and Planetary Interiorsen
dc.relation.ispartofseries/274 (2018)en
dc.subjectGutenberg-Richter modelen
dc.subjectCharacteristic earthquake modelen
dc.subjectProbabilistic Seismic Hazard Analysisen
dc.titleComments on ‘Why is Probabilistic Seismic Hazard Analysis (PSHA) still used?’ by F. Mulargia, P.B. Stark and R.J. Gelleren
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber214-215en
dc.identifier.doi10.1016/j.pepi.2017.09.009en
dc.description.obiettivoSpecifico6T. Studi di pericolosità sismica e da maremotoen
dc.description.journalTypeJCR Journalen
dc.contributor.authorConsole, Rodolfoen
dc.contributor.authorParsons, Tomen
dc.contributor.authorFalcone, Giuseppeen
dc.contributor.authorMurru, Mauraen
dc.contributor.authorYamashina, Ken'ichiroen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italiaen
dc.contributor.departmentU.S. Geological Survey, MS-999, 345 Middlefield Rd, Menlo Park, CA 94025, USAen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italiaen
dc.contributor.departmentEarthquake Research Institute (ERI), University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japanen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptU.S. Geological Survey, MS-999, 345 Middlefield Rd, Menlo Park, CA 94025, USA-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptEarthquake Research Institute (ERI), University of Tokyo, Yayoi 1-1-1, Bunkyo-ku, Tokyo 113-0032, Japan-
crisitem.author.orcid0000-0002-0582-4338-
crisitem.author.orcid0000-0002-2554-4421-
crisitem.author.orcid0000-0002-7385-394X-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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